Sea-level and ocean-current control on carbonate-platform growth, Maldives, Indian Ocean

Author:

Betzler Christian1,Fürstenau Jörn1,Lüdmann Thomas1,Hübscher Christian1,Lindhorst Sebastian1,Paul Andreas2,Reijmer John J. G.2,Droxler André W.3

Affiliation:

1. Department of Geosciences; University of Hamburg; Hamburg; Germany

2. Department of Sedimentology and Marine Geology; VU University Amsterdam; Amsterdam; The Netherlands

3. Department of Earth Science MS-126; Rice University; Houston; TX; USA

Publisher

Wiley

Subject

Geology

Reference65 articles.

1. SONIC VELOCITY IN CARBONATES—A COMBINED PRODUCT OF DEPOSITIONAL LITHOLOGY AND DIAGENETIC ALTERATIONS

2. From the Great Bahama Bank into the Straits of Florida: a Margin Architecture Controlled by Sea-Level Fluctuations and Ocean Currents;Anselmetti;Geol. Soc. Am. Bull.,2000

3. General cenozoic evolution of the Maldives carbonate system (equatorial Indian Ocean);Aubert;Bull. Centres Rech. Explor.-Prod. Elf-Aquitaine,1992

4. Seismic stratigraphy and depositional signatures of the Maldive carbonate system (Indian Ocean);Aubert;Mar. Pet. Geol.,1996

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